mineral

Polished rose quartz tower

Quartz, silicon dioxide (SiO₂), pink variety

AI-generated identification · may be incorrect

Mohs hardness 7; translucent pink to peach coloration, vitreous luster, and massive rather than visibly crystalline texture. Quartz has trigonal crystal structure, no cleavage, conchoidal fracture, and specific gravity about 2.65.

Identified September 4, 2026More mineral →

Explore Polished rose quartz tower in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

App Store Google Play

Physical properties

Formation & geological history

Rose quartz forms mainly in granitic pegmatites and hydrothermal veins, with color caused by trace elements and microscopic inclusions. The pictured tower is cut and polished, so its precise geological age and locality cannot be determined.

Uses & applications

Used for ornamental carvings, cabochons, beads, meditation objects, and mineral collecting; it has limited industrial value compared with clear quartz. Quality is judged by even color, translucency, and lack of fractures.

Geological facts

Rose quartz commonly shows cloudy, soft pink tones rather than the vivid transparency of many gemstones. Some specimens exhibit asterism when cut as cabochons.

Field identification & locations

Identify it by its pink massive quartz appearance, glassy polish, hardness, and inability to scratch with a steel knife; glass or calcite may resemble it but are softer. Common sources include Brazil, Madagascar, India, and South Africa.